Published August 29, 2019
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Text-fig. 5. (a) Examples of non-pervasive silicification of echinoderm remains. Interval 340–350 cm above the base of the section. (b) Moderately well-sorted peloidal grainstone with crinoid ossicles. Loose pilot sample Hýskov 2016-C. (c) Micritized grains in peloidal grainstone, note cluster of Girvanella in the center. Loose pilot sample Hýskov 2016-C. (d) Abraded clasts derived from calcareous green algae. Interval 40–50 cm above the base of the section. (e) Examples of non-pervasive silicification of echinoderm remains. 130 cm above the base of the section. (f) Articulated sponge skeleton. 130 cm above base of the section. in Llandovery Microfossils And Microfacies Of The Hýskov Section, Prague Basin
Creators
- 1. Czech Geological Survey, Klárov 3, 118 21 Prague 1, the Czech Republic; e-mail: petra.tonarova@geology.cz, stanislava.vodrazkova@geology.cz, michal.kubajko@geology.cz, jiri.fryda@geology.cz.
- 2. Department of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; e-mail: olle.hints@taltech.ee, peep.mannik@taltech.ee.
Description
Text-fig. 5. (a) Examples of non-pervasive silicification of echinoderm remains. Interval 340–350 cm above the base of the section. (b) Moderately well-sorted peloidal grainstone with crinoid ossicles. Loose pilot sample Hýskov 2016-C. (c) Micritized grains in peloidal grainstone, note cluster of Girvanella in the center. Loose pilot sample Hýskov 2016-C. (d) Abraded clasts derived from calcareous green algae. Interval 40–50 cm above the base of the section. (e) Examples of non-pervasive silicification of echinoderm remains. 130 cm above the base of the section. (f) Articulated sponge skeleton. 130 cm above base of the section.
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Related works
- Is part of
- Journal article: 10.2478/if-2019-0002 (DOI)
- Journal article: urn:lsid:plazi.org:pub:2C282F65FF89CA2BFFE85A1EFFF62D79 (LSID)
- Journal article: https://zenodo.org/record/4586631 (URL)